2016
DOI: 10.1190/geo2015-0069.1
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A fast algorithm for sparse multichannel blind deconvolution

Abstract: We have addressed blind deconvolution in a multichannel framework. Recently, a robust solution to this problem based on a Bayesian approach called sparse multichannel blind deconvolution (SMBD) was proposed in the literature with interesting results. However, its computational complexity can be high. We have proposed a fast algorithm based on the minimum entropy deconvolution, which is considerably less expensive. We designed the deconvolution filter to minimize a normalized version of the hybrid l 1 ∕l 2 -nor… Show more

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Cited by 34 publications
(18 citation statements)
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“…For this test, 20 traces are generated with a sampling frequency of 500 Hz using the reflectivity shown in Figure 1b, which can be downloaded from [29]. The received data 1 In equation (16) of [17] there is a typo for the k-th component of ∇L, which should be in Figure 1c is the convolution of the reflectivity with a Ricker wavelet of center frequency 40 Hz with 50 degrees of phase shift (see Figure 1a) plus additive white Gaussian noise (AWGN) of SNR = 10 dB. The SNR adopted in this work for the signal-plus-noise model, i.e., x = s + n is defined as SNR = 10 log 10 s 2…”
Section: Synthetic Data Testmentioning
confidence: 99%
See 1 more Smart Citation
“…For this test, 20 traces are generated with a sampling frequency of 500 Hz using the reflectivity shown in Figure 1b, which can be downloaded from [29]. The received data 1 In equation (16) of [17] there is a typo for the k-th component of ∇L, which should be in Figure 1c is the convolution of the reflectivity with a Ricker wavelet of center frequency 40 Hz with 50 degrees of phase shift (see Figure 1a) plus additive white Gaussian noise (AWGN) of SNR = 10 dB. The SNR adopted in this work for the signal-plus-noise model, i.e., x = s + n is defined as SNR = 10 log 10 s 2…”
Section: Synthetic Data Testmentioning
confidence: 99%
“…In seismic applications, conventional multichannel methods cannot be applied directly. The major cause is the great similarity between neighboring reflectivity sequences, which makes the problem either numerically sensitive or, at worst, ill-posed and impossible to solve [17].…”
Section: Introductionmentioning
confidence: 99%
“…Severe non-uniqueness issues are inherent to BD; there could be many possible g i and s pairs whose convolution will result in the observed data. In order to alleviate these non-uniqueness issues, recent BD algorithms in geophysics: 1. take advantage of the multichannel nature of the seismic data (Kaaresen and Taxt, 1998;Kazemi and Sacchi, 2014;Nose-Filho et al, 2015;Liu et al, 2016); 2. sensibly choose the initial estimates of the g i in order to converge to a desired solution (Liu et al, 2016); and/or 3. constrain the sparsity of the g i (Kazemi and Sacchi, 2014). Kazemi et al (2016) used sparse multichannel BD to estimate source and receiver wavelets while processing land seismic data.…”
Section: Introductionmentioning
confidence: 99%
“…Neste contexto, os algoritmos de busca baseados no gradiente, comumente utilizados para a obtenção dos coeficientes de um filtro de desconvolução [7], são bastante dependentes da inicialização, normalmente ficando presos em soluções subotimas. Para estas situações, o uso de algoritmos evolutivos torna-se uma opção bastante atraente.…”
Section: Introductionunclassified